963 resultados para Porto Ferreira (SP) - Educação, 1960-1980


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Pós-graduação em Educação - FFC

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O presente estudo foi realizado na Escola do Meio Ambiente (EMA) (22° 55' 23 S e 48° 27' 28 W), localizada a cinco km do centro do município de Botucatu. Foi realizado o levantamento preliminar da ictiofauna e dos invertebrados habitantes de uma represa de pequeno porte, inserida no perímetro da escola. Visando investigar os conhecimentos prévios dos alunos que realizam a Trilha da água, referentes às espécies habitantes do reservatório do Ribeirão Lavapés, 356 questionários foram aplicados aos alunos dos 6ºs anos e 150 questionários aos dos 2ºs anos de três escolas municipais de Botucatu. Quatro espécies de peixes e uma do grupo dos invertebrados foram coletadas. A análise dos questionários demonstrou o desconhecimento dos alunos em relação à fauna local. Este trabalho apresenta as etapas para a construção de um material didático, de apoio ao professor visitante da Trilha da Água, o qual aborda a fauna de peixes e invertebrados que habitam um açude pertencente à Escola do Meio Ambiente

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A inatividade física é uma das principais causas de morte no mundo, e um dos principais fatores de risco para doenças não transmissíveis. Os fatores de risco destas doenças podem ser prevenidos com modificações no estilo de vida, que reduz eventos cardiovasculares e aumenta a sobrevida de pacientes portadores ou em risco de coronariopatias. Entendendo de como estes agentes casuais se predispõem ao surgimento de cardiopatias, o acompanhamento de fatores de risco ajudam na identificação de sinais antecessores à doença, que podem ser modificados, atenuados e até mesmo revertidos. O objetivo do presente estudo foi de verificar a influência de um ano de prática regular de Atividade Física nas variáveis bioquímicas (bioquímicas (glicose, triglicérides, HDL, LDL, e colesterol total), circunferência de quadril e abdominal e Indice de Massa Corporal (IMC) de seus praticantes. Participaram do presente estudo 25 mulheres com idade superior a 40 anos participantes iniciantes do Programa de Exercício Físico na Atenção Básica da cidade de Rio Claro-SP. As atividades foram realizadas com frequência de três vezes por semana, em sessões de 60 minutos. Foram realizadas três análises laboratoriais (início, após 4 meses e um ano de intervenção) das variáveis bioquímicas (glicose, triglicérides, HDL, LDL, e colesterol total). Os principais resultados do presente estudo demonstraram que após quatros meses de intervenção a circunferência abdominal e o LDL apresentaram menores valores do que no início do programa. Entretanto, após um ano de intervenção a circunferência do quadril, abdominal, LDL, glicose e colesterol total apresentaram maiores valores do que quando comparado com os valores após os 4 meses. Com base nos resultados antropométricos percebe-se que houve melhores resultados aos quatro meses de intervenção do que com um ano de intervenção. Provavelmente o que ocorreu no caso do presente estudo se deve pela...

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Pós-graduação em Serviço Social - FCHS

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Within the current context of environmental degradation, primarily caused by unsustainable pat terns of production and consumption (AGENDA 21, 1992), the Protected Areas (PAs) are considered internationally as one of the most successful measures for the conservat ion of biodiversity, according to the Union for the Conservation of Nature (IUCN). The city of Rio Claro (Sao Paulo, Brazi l ) has a significant conservation area in both environmental aspects as historical and cultural, the State Forest 'Edmundo Navarro de Andrade' (FEENA). Beyond the conservation measures, there is a need to develop environmental education that encourages community participation and appreciation in the unit 's maintenance and protection, as well as provide moments of reflection that could conduct perceptual changes, behavioral, attitudinal and evaluative on relations between human beings and their environment . This work brings the proposal to create an interpretive trail in the area of public use of FEENA to contribute to the Unit Management Plan in order to make it an Environmental Education tool. To prepare the planning of the interpretive trail, a deep bibliographic and cartographic review was performed on the subject. It was applied questionnaires in order to know the visitors better and map the features of public visitation, as well as map the visitor preferences about how they would like to receive information on the area and expose field studies in the track site. The trail was traced taking into account the environmental and social aspects, we propose a track suspended above the ground, in order to affect as little as possible and to include the area in the context of PAs people with reduced mobility and visually impaired

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This research introduces subsidies to the composition of the Environmental Education Program of FEENA, specifically the implantation of an Educator Seedling Nursery. It consists in a lecture of the FEENA's landscape, essential to understand its current situation, and there are elements that will aid in the composition of the Program

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Pós-graduação em Serviço Social - FCHS

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This work investigates the behavior of the sunspot number and Southern Oscillation Index (SOI) signal recorded in the tree ring time series for three different locations in Brazil: Humaita in Amaznia State, Porto Ferreira in So Paulo State, and Passo Fundo in Rio Grande do Sul State, using wavelet and cross-wavelet analysis techniques. The wavelet spectra of tree ring time series showed signs of 11 and 22 years, possibly related to the solar activity, and periods of 2-8 years, possibly related to El Nio events. The cross-wavelet spectra for all tree ring time series from Brazil present a significant response to the 11-year solar cycle in the time interval between 1921 to after 1981. These tree ring time series still have a response to the second harmonic of the solar cycle (5.5 years), but in different time intervals. The cross-wavelet maps also showed that the relationship between the SOI x tree ring time series is more intense, for oscillation in the range of 4-8 years.

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This article examines the relations between the Turkish State Planning Organisation (SPO) and the Western economic system during the first two decades of national planning in Turkey (1960-1980). It traces how the SPO, established with the guidance and full endorsement of international economic institutions came to vehemently oppose Turkish participation in one of their pillars: the European Economic Community (EEC), the predecessor of the European Union. It argues that the shift in the SPO's world-view was founded upon two distinct understandings of the Turkish nation and its development, situates these understandings within the intellectual history of Turkey's past ambivalence towards the West, and, in doing so, provides a historical case-study of the ideological clash between modernisation and dependency theories of development.

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This report contains the occurrence data for dinoflagellate cysts recorded from 163 samples taken from Sites 902 through 906, during Ocean Drilling Program (ODP) Leg 150. The dinoflagellate cyst (dinocyst) stratigraphy has been presented in Mountain, Miller, Blum, et al. (1994, doi:10.2973/odp.proc.ir.150.1994), and was based on these data. This report provides the full dinocyst data set supporting the dinocyst stratigraphic interpretations made in Mountain, Miller, Blum, et al. (1994). For Miocene shipboard dinocyst stratigraphy, I delineated 10 informal zones: pre-A, and A through I, in ascending stratigraphic order. These zones are defined in Shipboard Scientific Party (1994a, doi:10.2973/odp.proc.ir.150.103.1994), and are based on my studies of Miocene dinocyst stratigraphy in the Maryland and Virginia coastal plain (de Verteuil and Norris, 1991, 1992; de Verteuil, 1995). This zonation has been slightly revised (de Verteuil and Norris, 1996), and the new formal zone definitions are repeated below. Each new zone has an alpha-numeric abbreviation starting with "DN" (for Dinoflagellate Neogene). The equivalence between the informal zones reported in Mountain, Miller, Blum, et al. (1994), and the new DN zones is illustrated in Figure 1. For clarity, I delineated both zonations in the range charts that accompany this report (Tables 1-6). De Verteuil and Norris (1996a), using these and other data, correlated the DN zonation with the geological time scale of Berggren et al. (1995). Figure 2 summarizes these correlations and can be used to check the chronostratigraphic position of samples in this report, as determined by dinocyst stratigraphy. A thorough discussion of the basis for, and levels of uncertainty associated with, these correlations to the Cenozoic time scale can be found in de Verteuil and Norris (1996a). The Appendix lists all the dinocyst taxa recorded during shipboard analyses of Leg 150 samples. Open nomenclature is used for undescribed taxa. The range charts and Appendix also include reference to several new taxa that de Verteuil and Norris (1996b) described from Miocene coastal plain strata in Maryland and Virginia. Names of these taxa in Tables 1 through 6 and in the Appendix of this report are not intended for effective publication as defined in the International Code of Botanical Nomenclature (ICBN, Greuter et al., 1994). Therefore, taxonomic nomenclature contained in this report is not to be treated as meeting the conditions of effective and valid publication (ICBN; Article 29).

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Photogrammetric surveys have been made and maps drawn of a number of glaciers in the eastern Alps, among them the Waxeggkees in the Zillertal Alps of Tyrol, at approximately ten-year intervals since 1950. Terrestrial photogrammetry was used for the pictures taken in 1950, 1960, 1980, 1989 and 2000, while aerial photogrammetry was employed for the 1969 photo. These maps were subsequently used to calculate the changes in area, elevation and volume for elevational zones of 50 m. The numeric values are given in two tables. The illustration of surface changes in Waxeggkees is continued cartographically on 5 map sheets at the scale of 1 : 15.000 and a vertical interval of the contour lines of 50 m. Changes in glacier area are marked in light red to indicate a decrease in area, and in light blue for an increase. Changes in elevation can only be indicated indirectly, namely in the form of vertical interval bands, referring to the surface areas that arise due to the relocation of the contour lines, resulting from an elevational change. Decrease in elevation is indicated in red, increase in blue, on 100 m contour lines.

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Climate variability and changes in the frequency of extremes events have a direct impact on crop damages and yield. In a former work of Capa et al. (2013) the crop yield variability has been studied using different reanalyses datasets with the aim of extending the time series of potential yield. The reliability of these time series have been checked using observational data. The influence of the sea surface temperature on the crop yield variability has been studied, finding a relation with El Niño phenomenon. The highest correlation between El Niño and yield was during 1960-1980. This study aims to analyse the dynamical mechanism of El Niño impacts on maize yield in Spain during 1960-1980 by comparison with atmospheric circulation patterns.